Features of the glacial history of the Transantarctic Mountains inferred from cosmogenic 26 Al, 10 Be and 21 Ne concentrations in bedrock surfaces
Abstract This paper describes measurements of concentrations of cosmogenic 26 Al, 10 Be and 21 Ne in quartz from bedrock surfaces in the Transantarctic Mountains where stratigraphic and geomorphic evidence shows that the surfaces were covered by ice in the past, but were not glacially eroded during...
Published in: | Antarctic Science |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
2014
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0954102014000261 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102014000261 |